The end of the rainy (Baiu) season in the Kanto region and northern Japan is induced by a "convection jump," known as the abrupt enhancement of convective activity (precipitation) over the northeast ...
More information: Ryouta Nakanishi et al, Summertime Convection Jump over the Subtropical Western North Pacific and its Relation to Rossby Wave Breaking near the Asian Jet Exit Region, Journal of ...
We aim to investigate cases where Rossby waves excited by local wind stress curl anomaly ... consistent with the argument of weak planetary wave dispersion. Figure 10C provides further details on ...
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It was all happening in big Rossby loops that had taken over the entire ... seven stalled peaks and lows over the same regions – ‘wave-7’ – has lasted seven times for more than two weeks.